Magmatic-hydrothermal redox state and ore-controlling factors for the Yangla skarn Cu deposit, Sanjiang region, SW China

Author:

Deng Ju-Ting,Zhu Jing-JingORCID,Hu Ruizhong,Hollings Pete,Bi Xian-Wu,Huang Ming-Liang,Yang Zong-Yong,Pan Li-Chuan,Wang Dian-Zhong

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference85 articles.

1. The solubility of Cu, Ag and Au in magmatic sulfur-bearing fluids as a function of oxygen fugacity;Alex;Geochim. Cosmochim. Acta,2022

2. The Metal Content of Magmatic-Hydrothermal Fluids and Its Relationship to Mineralization Potential;Audétat;Econ. Geol.,2019

3. Magmatic controls on porphyry Cu genesis. In (eds Hedenquist, J.W., et al.) Geology and Genesis of Major Copper Deposits and Districts of the World: A Tribute to Richard Sillitoe;Audétat;Soc. Econ. Geol Spec. Publ.,2012

4. Relative oxidation states of magmas inferred from Ce(IV)/Ce(III) in zircon: application to porphyry copper deposits of northern Chile;Ballard;Contrib. Miner. Petrol.,2002

5. Redox states and genesis of Cu- and Au-mineralized granite porphyries in the Jinshajiang Cu–Au metallogenic belt, SW China: studies on the zircon chemistry;Bao;Miner. Petrol.,2023

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